Geologists: scientist who study the forces that make and shape the Earth Rock: the material that forms most of the Earth's surface Geology: the study of Earth Constructive forces: forces that shape the surface by building up mountains and landmasses Destructive forces: forces that slowly wear away mountains and, eventually, every other feature on the surface Continents: the seven great landmasses on Earth Seismic waves: are produced when earthquakes occur Pressure: the pushing on a surface or area Crust: a layer of rock that forms Earth's outer skin
- Basalt: a dark, dense rock with a fine texture (usually found in oceanic crust)
- Granite: a rock that has larger crystals than basalt (usually found in continental crust) Mantle: a layer of hot rock between the crust and above the core Lithosphere: a rigid layer that contains the crust and the uppermost part of the mantle Asthenosphere: a soft layer under the lithosphere ( the material can flow easily in this layer) Outer core: a layer of molten metal that surrounds the inner core
Innercore: a dense ball of soled metal
Outline
The Science of Geology
studying surface changes
the surface is constantly changing
finding indirect evidence
we can't get to the middle of the Earth
instead of digging a hole we use seismic waves
Geologists record the seismic waves when an earthquake happens( they study the paths the waves take)
A Journey to the Center of the Earth
temperature changes
rocks are cool near the top
about 20 meters down, the rocks are getting warmer
the temperatures rises 1 Celsius ever 40 meters
that's pretty hot for the temperature down there
pressure also changes
as you go deeper the pressure increases
The Crust
There are two kinds of crusts
Oceanic Crust
the oceanic crust contains mostly basalt
darkly colored
Continental Crust
the continental crust contains mostly granite
lightly colored
The Mantle
the lithosphere contains part of the mantle
the lithosphere is about 100 kilometers thick
the asthenosphere is what the lithosphere floats on
the asthenosphere is the lowest part of the mantle
The Core
there are two parts that are called the "core"
The Outer Core
the outer core is a layer of molten metal
The Inner Core
extreme pressure squeezes the atoms of the iron so much they can't spread
the core makes about one third of Earth's mass but only 15 percent of its volume
Earth's Magnetic Field
the magnetic fields are created by the core
the inner core moves, this movement creates this field
the magnetic field causes the Earth to act like a big magnet bar
without the magnetic field, we would get burned from the sun's harmful rays (like the ultra violet rays)
Table of Contents
1.1 Earth's Interior
Vocabulary
Geologists: scientist who study the forces that make and shape the Earth
Rock: the material that forms most of the Earth's surface
Geology: the study of Earth
Constructive forces: forces that shape the surface by building up mountains and landmasses
Destructive forces: forces that slowly wear away mountains and, eventually, every other feature on the surface
Continents: the seven great landmasses on Earth
Seismic waves: are produced when earthquakes occur
Pressure: the pushing on a surface or area
Crust: a layer of rock that forms Earth's outer skin
- Basalt: a dark, dense rock with a fine texture (usually found in oceanic crust)
- Granite: a rock that has larger crystals than basalt (usually found in continental crust)
Mantle: a layer of hot rock between the crust and above the core
Lithosphere: a rigid layer that contains the crust and the uppermost part of the mantle
Asthenosphere: a soft layer under the lithosphere ( the material can flow easily in this layer)
Outer core: a layer of molten metal that surrounds the inner core
Inner core: a dense ball of soled metal
Outline
The Science of Geology
A Journey to the Center of the Earth
The Crust
The Mantle
The Core
Earth's Magnetic Field
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